Respostas do microplâncton marinho durante os Eventos Anóxicos Oceânicos (OAEs) do Cretáceo

Autores

DOI:

https://doi.org/10.11606/issn.2316-9095.v25-227385

Palavras-chave:

Produtividade marinha, Eventos de extinção, Taxa de rotatividade de espécies, Nanofósseis calcários, Oceano Atlântico Sul

Resumo

Os microfósseis desempenham um papel vital como componentes das rochas sedimentares depositadas durante o Cretáceo, fornecendo informações para a caracterização dos Eventos Anóxicos Oceânicos (OAEs). Esse estudo visa identificar e sistematizar as respostas do microplâncton marinho aos OAEs do Cretáceo, por meio da literatura publicada. Os microfósseis marinhos respondem aos OAEs por meio de eventos evolutivos, variações preservacionais, nas abundâncias e diversidade das associações. Além disso, esses organismos exportam concentrações significativas de elementos químicos para o fundo marinho, impactando o clima global. Mudanças nos ciclos orbitais do planeta e eventos paleogeográficos e vulcânicos de grande escala são considerados as principais causas que promoveram mudanças significativas nos ecossistemas do Mesozoico, resultando nos processos geológicos que caracterizam os OAEs. Ao analisar os oito OAEs do Cretáceo foi possível caracterizar as respostas geoquímicas e do microplâncton marinho para cada OAE. Por meio desse estudo é possível inferir que cada OAE possui características únicas, amplitude específica no tempo geológico, distintos fatores causais e impactos específicos sobre a biota marinha. Os microfósseis marinhos, em especial os nanofósseis calcários, radiolários e foraminíferos representam um importante componente para os ciclos biogeoquímicos do planeta e sua evolução está intimamente relacionada aos OAEs. Estudos adicionais, com materiais do Oceano Atlântico Sul, são necessários para melhor compreender os impactos dos OAEs na evolução da biota marinha.

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2025-06-03

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Bruno, M. D. R., Tungo, E. D. J. F., Luft-Souza, F., Sander, V. H., & Fauth, G. (2025). Respostas do microplâncton marinho durante os Eventos Anóxicos Oceânicos (OAEs) do Cretáceo. Geologia USP. Série Científica, 25(2), 3-32. https://doi.org/10.11606/issn.2316-9095.v25-227385

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